The climate of the Earth follows a complex interplay of cause-and-effect chains. A change in precipitation at one location may be caused by changes on the other side of the planet. A better understanding of these “teleconnections” – the linkages between remote places – may help to better understand local impacts of future climate change. A look into the climate of the past helps to investigate the teleconnections. An international team of Japanese, British, Australian, and German scientists, with the participation of the GFZ German Research Centre for Geosciences, now investigated Japanese lake sediments to decipher the interplay between local climate changes on the northern hemisphere about 12.000 years ago. Their results, now published as Nature Scientific Report, show that a regional warming in Europe caused a cooling and an increase in snowfall in East Asia.
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